Ceramic polymers or "geopolymers" are amorphous to semi-crystalline three dimensional alumino-silicate materials resulting from geochemistry. "Geopolymerisation" is the chemical reaction between various aluminosilicate oxides (Al+3 in Iv, V, or Vi fold coordination) with silicates under highly alkaline conditions, yielding polymeric Si-O-Al-O bonds (HUA & VanDeventer 1999). Geopolymers form co-polymerisation of individual alumino and silicate species, which originate from materials containing host sources of either silicon, aluminum or combinations of the foregoing. In order to form geopolymer chains, rings or complete tetrahedral, positive ions such as K, Na, Ca, Ba, Nhy, H30 (etc) must be present in the framework in order to balance the negative charge of Al. Differing chain and ring structures form at different Si: Al ratios. Polymeric structures are generally formed when the Si:Al ratio is greater than 3. From this polysilicate chains can form 3-dimensional cross-linked structures. It is this cross-linking phenomenon which facilitates the ability to enhance the standard characteristics of traditional ceramics yielding ceramic polymers (geopolymers)which are characterized by
Keywords: Ceramic, Polymer, Geopolymerization, Alumino-Silicate, Durability, Stability, Transformation, Toughening